<?xml version="1.0" encoding="UTF-8"?><xml><records><record><source-app name="Biblio" version="6.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Zhou, T. J.</style></author><author><style face="normal" font="default" size="100%">Yu, R. C.</style></author><author><style face="normal" font="default" size="100%">Zhang, J.</style></author><author><style face="normal" font="default" size="100%">Drange, Helge</style></author><author><style face="normal" font="default" size="100%">Cassou, C.</style></author><author><style face="normal" font="default" size="100%">Deser, C.</style></author><author><style face="normal" font="default" size="100%">Hodson, D. L. R.</style></author><author><style face="normal" font="default" size="100%">et al</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Why the Western Pacific Subtropical High Has Extended Westward since the Late 1970s</style></title><secondary-title><style face="normal" font="default" size="100%">Journal of Climate</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2009</style></year></dates><urls><related-urls><url><style face="normal" font="default" size="100%">http://www.nersc.no/sites/www.nersc.no/files/2008jcli2527%2E1.pdf</style></url></related-urls></urls><number><style face="normal" font="default" size="100%">8</style></number><volume><style face="normal" font="default" size="100%">22</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><section><style face="normal" font="default" size="100%">2199-2215</style></section><auth-address><style face="normal" font="default" size="100%">NERSC</style></auth-address></record></records></xml>